1 Formation
1.1 Formation
The banded iron layers are formed in sea water when oxygen is released by photosynthetic cyano-bacteria. The oxygen then combines with dissolved iron in ocean to form insoluble iron oxides, which precipitated out, forming a thin layer of banded iron formation on ocean floor.
Chalk is formed from lime mud, which accumulates on the sea floor which is then transformed into rock by geological processes.
1.2 Composition
1.2.1 Mineral Content
Hematite, Magnetite, Quartz
Calcite, Clay, Clay Minerals, Quartz, Sand
1.2.2 Compound Content
Fe, Iron(III) Oxide, Silicon Dioxide
Ca, NaCl, CaO
1.3 Transformation
1.3.1 Metamorphism
1.3.2 Types of Metamorphism
Not Applicable
Not Applicable
1.3.3 Weathering
1.3.4 Types of Weathering
Chemical Weathering
Biological Weathering, Chemical Weathering
1.3.5 Erosion
1.3.6 Types of Erosion
Coastal Erosion, Wind Erosion
Chemical Erosion, Coastal Erosion, Water Erosion